Zeolitization of Miocene dacitic tuffs in the Janggi Basin, Korea: influence of depositional conditions and fluid system evolution

Key Points

• Zeolitization occurs in Miocene dacitic tuffs, indicating significant mineral transformation under specific conditions.
• Key evidence shows pore morphology changes in relation to fluid system evolution, affecting overall deposits.
• Observational analysis of mineralogical changes highlights the role of depositional conditions over time with fluid interactions.
• Results suggest implications for understanding geological processes and mineral formation in similar environments.